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Aleutian low

[ uh-loo-shuhn loh ]

noun

, Meteorology.
  1. a semipermanent, subarctic system of low atmospheric pressure in the Gulf of Alaska, near the Aleutian Islands, a storm-breeding area from late fall into late spring, as migratory lows often reach maximum intensity there: as the Aleutian low becomes weakened and displaced toward the North Pole with the onset of summer, the North Pacific high becomes more dominant.


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Word History and Origins

Origin of Aleutian low1

First recorded in 1910–15
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Example Sentences

The great storm-breeder, the Aleutian Low, is watched from Alaskan shores.

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Aleutian IslandsAleutian Range